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From such considerations are derived the differential equations that describe fluid motion (see fluid mechanics).
Deriving analytical expressions to describe fluid flow in porous medium is a complex task.
In this section, comparisons and a field example are presented to describe fluid flow in NFTRs.
In this paper, we use and discuss Couette equation to describe fluid flow in natural fractures.
Kazemi et al. (1976) introduced the dual-porosity model into numerical model to describe fluid flow on large scale.
Following this method simplifies the incorporation of discontinuities without requiring developing a whole new system to describe fluid flow.
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In subsequent decades, physicists developed theories to describe fluids at high densities.
Statistical physicists describe fluids with scaling laws, equations that describe how the physical properties of a fluid change near a so-called critical point.
A unique formulation of describing fluid motion is presented.
Helmholtz knew of Euler's and Lagrange's previous mathematical formulas describing fluid motion.
Hence this approach unifies the two classical methods for describing fluid flows.
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